The large impact hypothesis is currently favored as explaining how the moon was formed. It proposes that a massive object collided with the early Earth, sending debris into orbit that eventually coalesced into the moon. After its formation, the moon was bombarded with asteroids and its low areas filled with lava, which cooled to form dark maria. The moon is littered with impact craters and has a geology defined by lighter colored highlands and darker lowlands and maria. While no life exists on the moon currently or historically, small amounts of water ice have been discovered frozen at its poles.